Deciphering topographic signals of glaciation and rock uplift in an active orogen: a case study from the Olympic Mountains, USA

• Published in: Earth Surface Processes and Landforms
• Main Authors: Adams, B. A., Ehlers, T. A.
• Other Authors: European Research Council
• Format: Article in Journal/Newspaper
• Language: English
• Published: Wiley 2017
• Subjects: Ice Sheet
• Online Access: http://dx.doi.org/10.1002/esp.4120; https://api.wiley.com/onlinelibrary/tdm/v1/articles/10.1002%2Fesp.4120; https://onlinelibrary.wiley.com/doi/pdf/10.1002/esp.4120

Abstract Estimating recent patterns of erosion and rock uplift within Cenozoic orogens has proven difficult as signals of these processes have been obfuscated by Plio‐Pleistocene glaciation. The topography of many mountain ranges integrates the effects of long‐lived rock uplift, Late‐Cenozoic climate variation, and post‐glacial landscape adjustment. In this study, we employ a suite of topographic analyses to study the relief of an active mountain range on a sub‐catchment scale in an effort to the separate the long‐term signal of rock uplift from perturbations due to shorter‐lived climate signals. We focus on the Olympic Mountains, USA, where patterns of exhumation and glaciation have been previously estimated; however, our methods and results are broadly applicable to other orogens. Our analysis shows that Plio‐Pleistocene alpine glaciers and the Cordilleran Ice Sheet have reduced the elevations of channel profiles and created anomalously low channel relief in the Olympic Mountains. Large low‐gradient areas formed at lower elevations where ice sheets were present and alpine glaciers widened and deepened valleys. In the more rugged core of the range, near‐threshold hillslopes along the margins of the oversteepened glacially‐carved valleys, dominate the range. This implies a strong Plio‐Pleistocene glacial climate control on the topography over the more recent evolution of the Olympic Mountains. However, the broad relief structure of the range appears to still record the regional rock uplift pattern and is suggestive of an east‐plunging antiform, consistent with folding of the subducting plate or underplating of accreted rocks. Copyright © 2017 John Wiley & Sons, Ltd.